文献类型：期刊文献

英文题名：El Nino/Southern Oscillation during the 4.2 ka event recorded by growth rates of corals from the North South China Sea

作者：Dang, Shaohua[1,2,3];Yu, Kefu[1,2,3];Tao, Shichen[4];Han, Tao[4];Zhang, Huiling[5];Jiang, Wei[1,2,3]

机构：[1]Guangxi Univ, Guangxi Lab Study Coral Reefs South China Sea, Nanning 530004, Peoples R China;[2]Guangxi Univ, Coral Reef Res Ctr China, Nanning 530004, Peoples R China;[3]Guangxi Univ, Sch Marine Sci, Nanning 530004, Peoples R China;[4]Chinese Acad Sci, South China Sea Inst Oceanol, Guangzhou 510301, Peoples R China;[5]Guangdong Ocean Univ, Coll Ocean Engn, Zhanjiang 524088, Peoples R China

年份：2020

卷号：39

期号：1

起止页码：110

外文期刊名：ACTA OCEANOLOGICA SINICA

收录：SCI-EXPANDED(收录号：WOS:000519120000011)、、WOS

基金：The National Natural Science Foundation of China under contract No. 91428203; the Guangxi Scientific Projects under contract Nos AD17129063 and AA17204074; the Bagui Fellowship from Guangxi of China.

语种：英文

外文关键词：4.2 ka event; ENSO variability; SSTA; coral growth rate; Xisha Islands

外文摘要：The 4.2 ka event that occurred during the period from 4 500-3 900 a BP was characterized by cold and dry climates and resulted in the collapse of civilizations around the world. The cause of this climatic event, however, has been under debate. We collected four corals (Porites lutea) from Yongxing Island, Xisha Islands, South China Sea, dated them with the U-series method, and measured the annual coral growth rates using X-ray technology. The dating results showed that the coral growth ages were from 4 500-3 900 a BP, which coincide well with the period of the 4.2 ka event. We then reconstructed annual sea surface temperature anomaly (SSTA) variations based on the coral growth rates. The growth rate-based SSTA results showed that the interdecadal SSTA from 4 500-3 900 a BP was lower than that during modern times (1961-2008 AD). A spectral analysis showed that the SSTA variations from 4 500-3 900 a BP were under the influence of El Nino-Southern Oscillation (ENSO) activities. From 4 500-4 100 a BP, the climate exhibited La Nina-like conditions with weak ENSO intensity and relatively stable and lower SSTA amplitudes. From 4 100-3 900 a BP, the climate underwent a complicated period of ENSO variability and showed alternating El Nino- or La Nina-like conditions at interdecadal time scales and large SSTA amplitudes. We speculate that during the early and middle stages of the 4.2 ka event, the cold climate caused by weak ENSO activities largely weakened social productivity. Then, during the end stages of the 4.2 ka event, the repeated fluctuations in the ENSO intensity caused frequent extreme weather events, resulting in the collapse of civilizations worldwide. Thus, the new evidence obtained from our coral records suggests that the 4.2 ka event as well as the related collapse of civilizations were very likely driven by ENSO variability.